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Institutional investors are the biggest component of the so-called "smart money" group. There are generally six types of institutional investors: pension funds, endowment funds, insurance companies, commercial banks, mutual funds and hedge funds.
Most institutional investors in the U.S. are regulated by the Securities and Exchange Commission (SEC). Institutional investors must file a Form 13F with the SEC to report their quarterly holdings; they must also file a Form 13G if they own more than 5% of a company's stock. Retail investors can use these public filings to peek into what institutions are buying or selling each quarter.
Institutional investors have the resources to do extensive research on wide-ranging investment options, and due to their specialized knowledge, they generally have an edge over retail investors. Portfolio managers often meet personally with company executives, study entire industries, and evaluate companies in depth before making specific investment decisions.

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lithosphereThe word lithosphere is derived from the word sphere, combined with the Greek word lithos, meaning rock . The lithosphere is the solid outer section of Earth, which includes Earth's crust (the "skin" of rock on the outer layer of planet Earth), as well as the underlying cool, dense, and rigid upper part of the upper mantle. The lithosphere extends from the surface of Earth to a depth of about 44–62 mi (70–100 km). This relatively cool and rigid section of Earth is believed to "float" on top of the warmer, non-rigid, and partially melted material directly below. Earth is made up of several layers. The outermost layer is called Earth's crust. The thickness of the crust varies. Under the oceans , the crust is only about 3–5 mi (5–10 km) thick. Under the continents, however, the crust thickens to about 22 mi (35 km) and reaches depths of up to 37 mi (60 km) under some mountain ranges. Beneath the crust is a layer of rock material that is also solid, rigid, and relatively cool, but is assumed to be made up of denser material. This layer is called the upper part of the upper mantle, and varies in depth from about 31–62 mi (50–100 km) below Earth's surface. The combination of the crust and this upper part of the upper mantle, which are both comprised of relatively cool and rigid rock material, is called the lithosphere. Below the lithosphere, the temperature is believed to reach 1,832°F (1,000°C), which is warm enough to allow rock material to flow if pressurized. Seismic evidence suggests that there is also some molten material at this depth (perhaps about 10%). This zone which lies directly below the lithosphere is called the asthenosphere , from the Greek word asthenes, meaning weak. The lithosphere, including both the solid portion of the upper mantle and Earth's crust, is carried "piggyback" on top of the weaker, less rigid asthenosphere, which seems to be in continual motion. This motion creates stress in the rigid rock layers above it, forcing the slabs or plates of the lithosphere to jostle against each other, much like ice cubes floating in a bowl of swirling water . This motion of the lithospheric plates is known as plate tectonics , and is responsible for many of the movements seen on Earth's surface today including earthquakes, certain types of volcanic activity, and continental drift.
Last Update:2016-02-21
Subject: Science
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Tagalog

lithosphereThe word lithosphere is derived from the word sphere, combined with the Greek word lithos, meaning rock . The lithosphere is the solid outer section of Earth, which includes Earth's crust (the "skin" of rock on the outer layer of planet Earth), as well as the underlying cool, dense, and rigid upper part of the upper mantle. The lithosphere extends from the surface of Earth to a depth of about 44–62 mi (70–100 km). This relatively cool and rigid section of Earth is believed to "float" on top of the warmer, non-rigid, and partially melted material directly below.
Earth is made up of several layers. The outermost layer is called Earth's crust. The thickness of the crust varies. Under the oceans , the crust is only about 3–5 mi (5–10 km) thick. Under the continents, however, the crust thickens to about 22 mi (35 km) and reaches depths of up to 37 mi (60 km) under some mountain ranges. Beneath the crust is a layer of rock material that is also solid, rigid, and relatively cool, but is assumed to be made up of denser material. This layer is called the upper part of the upper mantle, and varies in depth from about 31–62 mi (50–100 km) below Earth's surface. The combination of the crust and this upper part of the upper mantle, which are both comprised of relatively cool and rigid rock material, is called the lithosphere.
Below the lithosphere, the temperature is believed to reach 1,832°F (1,000°C), which is warm enough to allow rock material to flow if pressurized. Seismic evidence suggests that there is also some molten material at this depth (perhaps about 10%). This zone which lies directly below the lithosphere is called the asthenosphere , from the Greek word asthenes, meaning weak. The lithosphere, including both the solid portion of the upper mantle and Earth's crust, is carried "piggyback" on top of the weaker, less rigid asthenosphere, which seems to be in continual motion. This motion creates stress in the rigid rock layers above it, forcing the slabs or plates of the lithosphere to jostle against each other, much like ice cubes floating in a bowl of swirling water . This motion of the lithospheric plates is known as plate tectonics , and is responsible for many of the movements seen on Earth's surface today including earthquakes, certain types of volcanic activity, and continental drift.

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subjectivity, in this specifically humanist construction, was still perdicated on a model
of interior selfhood of identity as psychic depth, and these people invariably appeales to it
when they justifies their declarations of their own homosexuality as a search for authenticity.

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HOW DO I LOVE THEE
How do I love thee? Let me count the ways
I love thee to the depth and breadth and height
My soul can reach, when feeling out of sight
For the ends of Being and idela Grace
I love thee to the level of everyday’s
Most quiet need, by sun and candle-light
I love thee freely, as men strive for Right;
I love thee purely, as they turn from Praise
I love thee with a passion put to use
In my old griefs, and with my childhood’s faith
I love thee with a love I seemed to lose
With my lost saints, — I love thee with the breath,
Smiles, tears of all my life! – and, if God choose,
I shall but love thee better after death